Abstract
Understanding the response of aquifer thermal regime on different climatic events is important to predict the effects of climate change in groundwater aquifers. A heat transport model that incorporates the effect of groundwater flow was developed to estimate the seasonal heat flux change in the Sendai Plain. Domenico & Palciauskas's analytical solution for 2-D heat transport was used to investigate the heat flow during four months time period (From 01-May-2007 to 31-August-2007). Potential distribution of groundwater flow was simulated by means of the MODFLOW numerical code. Simulated results were verified with observed water level and temperature records at three observation wells. 47.5 mW/m2 of maximum vertical heat flux was estimated near to the Nanakita River and it also noticed about 17% heat flux change during two extreme precipitation events of simulation time.
| Original language | English |
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| Title of host publication | From Headwaters to the Ocean: Hydrological Changes and Watershed Management - Proceedings of the International Conference on Hydrological Changes and Management from Headwaters to the Ocean, HYDROCH |
| Pages | 329-335 |
| Number of pages | 7 |
| Publication status | Published - 2009 |
| Event | International Conference on Hydrological Changes and Management from Headwaters to the Ocean, HYDROCHANGE 2008 - Kyoto, Japan Duration: Oct 1 2008 → Oct 3 2008 |
Other
| Other | International Conference on Hydrological Changes and Management from Headwaters to the Ocean, HYDROCHANGE 2008 |
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| Country/Territory | Japan |
| City | Kyoto |
| Period | 10/1/08 → 10/3/08 |
Keywords
- Groundwater
- Heat flux
- MODFLOW
- Sendai Plain
- Temperature effect
ASJC Scopus subject areas
- Geochemistry and Petrology
- Ocean Engineering
- Water Science and Technology